28 Maxwell's equation and-2
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最伟大的数学公式排名数学公式是数学的基础,它们用于描述各种概念、关系和规律。
但是,要评价哪个数学公式最伟大是主观的,因为每个公式都有其独特的背景和重要性。
以下是一些被广泛认为是非常重要和有影响的数学公式。
1. 欧拉公式(Euler's formula):这个公式将三角函数、指数函数和复数关联起来,是数学中最重要的公式之一。
2. 牛顿-莱布尼兹公式(Newton-Leibniz formula):这个公式用于计算定积分,是微积分的基础。
3. 泰勒公式(Taylor series):这个公式用于展开函数,是分析数学的重要工具。
4. 欧拉-麦克劳林公式(Euler-Maclaurin formula):这个公式将欧拉和麦克劳林两种求和的方法结合起来,用于求和和积分。
5. 贝叶斯定理(Bayes' theorem):这个公式用于概率推理和统计推断,是贝叶斯方法的基石。
6. 傅里叶变换(Fourier transform):这个公式将时间和空间域上的函数转换为频率域上的函数,是信号处理和图像处理领域的基础。
7. 拉普拉斯变换(Laplace transform):这个公式将时间域上的函数转换为复平面上的函数,用于求解偏微分方程。
8. 欧拉-雅可比公式(Euler-Jacobi formula):这个公式用于求解变分问题,是优化理论和力学中的重要工具。
9. 麦克斯韦方程组(Maxwell's equations):这个方程组描述了电磁场的运动规律,是电动力学的基础。
10. 薛定谔方程(Schrödinger equation):这个方程描述了量子力学中微观粒子的运动状态,是量子力学的基础。
这些公式都是数学中的重要工具,对于不同的领域有着不同的影响和应用。
因此,无法简单地评价哪个公式最伟大,它们各自在数学和科学中扮演着重要的角色。
麦克斯韦电磁方程
麦克斯韦电磁方程,又称麦克斯韦方程,是20世纪初期热激励学派物理学家查尔斯特·麦克斯韦于1864年在他的著作《223课中对磁力学部分的建构》中提出的电磁学基本原理,它是电磁学中重要的基本公式,是把电磁学所有基础理论连接在一起的基础。
麦克斯韦电磁方程具有四个分支,分别是相对论电磁交互方程(Maxwell’s equations of the relativistic Electromagnetism)、非相对论电磁交互方程(Maxwell’s equations of the non-relativistic Electromagnetism)、伽马方程(the equation of gamma)以及静电场方程(the equation of electrostatic field)。
其中,四个麦克斯韦方程可以用一个总的式子描述:
\oint_\mathrm{c} \vec E \cdot d\vec l= - \frac{1}{c} \frac{\partial}{\partial t}\int_\mathrm{S}\vec B \cdot d\vec S 它由C积分表示,即分别表示某一点处的电场强度\vec E ,磁场强度\vec B ,磁环曲率c 以及时间t。
式中,只要存在选定曲线C 以及面积S,就能求出E 和B 的变化关系,即可求出相应空间处的传播速度c(光速)。
麦克斯韦方程表明电磁场和电流之间的联系,只要一定环境下存在电流,就会在相应空间形成电磁场;只要存在电磁场,就能在相应空间产生电流。
这也给把电磁理论应用到日常生活(例如电力、电磁机械)中提供了重要的理论基础,并且在磁波通信、高能物理学和天文学等许多领域有着深远的影响。
几年前英国科学期刊《物理世界》曾让读者投票评选了“最伟大的公式”,最终榜上有名的十个公式既有无人不知的1+1=2,又有著名的E=mc^2;既有简单的-圆周公式,又有复杂的欧拉公式……这些公式不仅仅是数学家和物理学家的智慧结晶,更是人类文明的集中体现。
每一个公式都深深影响了人类社会的变革,甚至塑造了人类的思想。
这些公式中有些你会很熟悉,有些你也许不那么熟悉。
作为人类的我们有必要了解这些公式,了解人类的思想历程。
对于电子工程师来说,傅里叶变换、麦克斯韦方程都是最应该了解和掌握的。
今天我们从网络收集整理了这10著名公式,分享给大家:No.10 圆的周长公式(The Length of the Circumference of a Circle)创立者:古人意义:自然界之美的数学表达。
这公式贼牛逼了,初中学到现在。
目前,人类已经能得到圆周率的2061亿位精度。
还是挺无聊的。
现代科技领域使用的-圆周率值,有十几位已经足够了。
如果用35位精度的-圆周率值,来计算一个能把太阳系包起来的一个圆的周长,误差还不到质子直径的百万分之一。
现在的人计算圆周率,多数是为了验证计算机的计算能力,还有就是为了兴趣。
No.9 傅立叶变换(The Fourier Transform)创立者:让·巴普蒂斯·约瑟夫·傅立叶意义:任何不规则的信号都可以表示为规则的正弦波无限叠加。
它是数字信号处理领域的很重要的方法。
这个挺专业的,一般人完全不明白。
不多作解释。
简要地说没有这个式子没有今天的电子计算机,所以你能在这里上网除了感谢党感谢政府还要感谢这个完全看不懂的式子。
另外傅立叶虽然姓傅,但是法国人。
No.8 德布罗意方程组(The de Broglie Relations)创立者:路易·维克多·德布罗意意义:德布罗意认为,任何物质既有粒子性,又有波动性,或者说,任何物质也可以看成是一种波,包括人本身。
目录PROPERTIES OF ANTENNAS . (1)1.1ANTENNA RADIATION (2)1.2GAIN . (4)1.3EFFECTIVE AREA (6)1.4PATH LOSS (7)1.5RADAR RANGE EQUATION AND CROSS SECTION (9)1.6WHY USE AN ANTENNA? (11)天线的性能. (12)1.1天线辐射 (13)1.2增益. (14)1.3有效面积 (16)1.4路径损耗 (17)1.5雷达距离方程和截面 (19)1.6为什么要使用一个天线? (20)英文原文:PROPERTIES OF ANTENNASOne approach to an antenna book starts with a discussion of how antennas radiate. Beginning with Maxwell 'es quations, we derive electromagnetic waves. After that lengthy discussion, which contains a lot of mathematics, we discuss how these waves excite currents on conductors. The second half of the story is that currents radiate and produce electromagnetic waves. You may already have studied that subject, or if you wish to further your background, consult books on electromagnetics.The study of electromagnetics gives insight into the mathematics describing antenna radiation and provides the rigor to prevent mistakes. We skip the discussion of those equations and move directly to practical aspects.It is important to realize that antennas radiate from currents. Design consists of controlling currents to produce the desired radiation distribution, called its pattern .In many situations the problem is how to prevent radiation from currents, such as in circuits. Whenever a current becomes separated in distance from its return current, it radiates. Simply stated, we design to keep the two currents close together, to reduce radiation. Some discussions will ignore the current distribution and instead, consider derived quantities, such as fields in an aperture or magnetic currents in a slot or around the edges of a microstrip patch. You will discover that we use any concept that provides insight or simplifies the mathematics.An antenna converts bound circuit fields into propagating electromagnetic waves and, by reciprocity, collects power from passing electromagnetic waves. Maxwell ' s equations p that any time-varying electric or magnetic field produces the opposite field and forms an electromagnetic wave. The wave has its two fields oriented orthogonally, and it propagates in the direction normal to the plane defined by the perpendicular electric and magnetic fields. The electric field, the magnetic field, and the direction of propagation form a right-handed coordinate system. The propagating wave field intensity decreasesb y 1/R away from the source, whereas a static field drops off by 1/R2. Any circuit with time-varying fields has the capability of radiating to some extent.We consider only time-harmonic fields and use phasor notation with time dependence e jwt. An outward-propagating wave is given by e j(kR wt), where k, the wave number, is given by 2 π / λ . λ is the wavelength of the wave given by c/f , where c is the velocity of light (38×10 m/s in free space) and f is the frequency. Increasing the distance from the source decreases thephase of the wave.Consider a two-wire transmission line with fields bound to it. The currents on a single wire will radiate, but as long as the ground return path is near, its radiation will nearly cancel the other line 's radiation becauseo tahree t1w80 ou°t of phase and the waves travel about thesame distance. As the lines become farther and farther apart, in terms of wavelengths, the fields produced by the two currents will no longer cancel in all directions. In some directions the phase delay is different for radiation from the current on each line, and power escapes from the line. We keep circuits from radiating by providing close ground returns. Hence, high-speed logic requires ground planes to reduce radiation and its unwanted crosstalk.1.1ANTENNA RADIATIONAntennas radiate spherical waves that propagate in the radial direction for a coordinate system centered on the antenna. At large distances, spherical waves can be approximated by plane waves. Plane waves are useful because they simplify the problem. They are not physical, however, because they require infinite power.The Poynting vector describes both the direction of propagation and the power density of the electromagnetic wave. It is found from the vector cross product of the electric and magnetic fields and is denoted S:2S = E H×* W/m2Root mean square (RMS) values are used to express the magnitude of the fields. H* is the complex conjugate of the magnetic field phasor. The magnetic field is proportional to the electric field in the far field. The constant of proportion is η , the impedance of free 376.73 Ω ):E 2 2S S W/ m2(1.1)Because the Poynting vector is the vector product of the two fields, it is orthogonal to both fields and the triplet defines a right-handed coordinate system: (E, H, S).Consider a pair of concentric spheres centered on the antenna. The fields around the 23antenna decrease as 1/R, 1R/ , 1/R , and so on. Constant-order terms would require that the power radiated grow with distance and power would not be conserved. For field terms 23proportional to 1/ R , 1/R , and higher, the power density decreases with distance faster thanthe area increases. The energy on the inner sphere is larger than that on the outer sphere. The energies are not radiated but are instead concentrated around the antenna; they are near-field 2terms. Only the 1/R term of the Poynting vector (1/R field terms) represents radiated power2because the sphere area grows as R and gives a constant product. All the radiated power flowingthrough the inner sphere will propagate to the outer sphere. The sign of the input reactance depends on the near-field predominance of field type: electric (capacitive) or magnetic (inductive). At resonance (zero reactance) the stored energies due to the near fields are equal. Increasing the stored fields increases the circuit Q and narrows the impedance bandwidth.Far from the antenna we consider only the radiated fields and power density. The powerflow is the same through concentric spheres:2The average power density is proportional to 1/R . Consider differential areas on the two spheres at the same coordinate angles. The antenna radiates only in the radial direction; therefore, no power may travel in the θ or φ direction. Power travels in flux tubes between areas, and it follows that not only the average Poynting vector but also every part of the power2density is proportional to 1/R :22S 1R 1 sin d d S 2R 2 sin d dSince in a radiated wave S is proportional to 1R / 2 , E is proportional to 1/R. It is convenient to define radiation intensity to remove the 1/R 2dependence: U(θ, φ ) = S(R, R θ2, φW) /solid angle Radiation intensity depends only on the direction of radiation and remains the same at all distances. A probe antenna measures the relative radiation intensity (pattern) by moving in a circle (constant R) around the antenna. Often, of course, the antenna rotates and the probe is stationary.Some patterns have established names. Patterns along constant angles of the spherical coordinates are called either conical (constant θ ) or great circle (constantφ ). Thcuts when φ = 0 ° or φ = 90 ° are the principal plane patterns. Other named cuts are also used, but their names depend on the particular measurement positioner, and it is necessary to annotate these patterns carefully to avoid confusion between people measuring patterns on different positioners. Patterns are measured by using three scales: (1) linear (power), (2)2 4 R 12S 1 ,avg 4 R 2 S 2, avgsquare root (field intensity), and (3) decibels (dB). The dB scale is used the most because it reveals more of the low-level responses (sidelobes).Figure 1.1 demonstrates many characteristics of patterns. The half-power beamwidth is sometimes called just the beamwidth. The tenth-power and null beamwidths are used in some applications. This pattern comes from a parabolic reflector whose feed is moved off the axis. The vestigial lobe occurs when the first sidelobe becomes joined to the main beam and forms a shoulder. For a feed located on theaxis of the parabola, the first sidelobes are equal. 1.2 GAINGain is a measure of the ability of the antenna to direct the input power into radiation in aparticular direction and is measured at the peak radiation intensity. Consider the power2 densityradiated by an isotropic antenna with input power Po at a distance R: S = Po/4 R . An isotropic antenna radiates equally in all directions, and its radiated power density S is found by dividing the radiated power by the area of thes phere 4 R π2. The isotropic radiator is considered to be 100% efficient. The gain of an actual antenna increases the power density in the direction of the peak radiation:Gain is achieved by directing the radiation away from other parts of the radiation sphere. Ingeneral, gain is defined as the gain-biased pattern of the antenna:SP 0GS 2 4 R 2 or (1.2)P 0G4 R 2 power densityP 0G , 4radiation intensity (1.3)1 4where Pr is the radiated power. Material losses in the antenna or reflected power due to poor impedance match reduce the radiated power. In this book, integrals in the equation above and those that follow express concepts more than operations we perform during design. Only for theoretical simplifications of the real world can we find closed-form solutions that would call for actual integration. We solve most integrals by using numerical methods that involve breaking the integrand into small segments and performing a weighted sum. However, it is helpful that integrals using measured values reduce the random errors by averaging, which improves the result.In a system the transmitter output impedance or the receiver input impedance may not match the antenna input impedance. Peak gain occurs for a receiver impedance conjugate matched to the antenna, which means that the resistive parts are the same and the reactive parts are the same magnitude but have opposite signs. Precision gain measurements require atuner between the antenna and receiver to conjugate-match the two. Alternatively, theP rP 0 2 G , sin d d 0 0 4 efficiencyFIGURE 1.1 Antenna pattern characteristics.The surface integral of the radiation intensity over the radiation sphere divided by the input power Po is a measure of the relative power radiated by the antenna, or the antennamismatch loss must be removed by calculation after the measurement. Either the effect ofmismatches is considered separately for a given system, or the antennas are measured into the system impedance and mismatch loss is considered to be part of the efficiency.Example Compute the peak power density at 10 km of an antenna with an input power of 3 W and a gain of 15 dB.1510First convert dB gain to a ratio: G = 10 10= 31.62. The power spreads over the sphere area with radius 10 km or an area of 4π(104 )2 m 2. The power density is 3W (31.62) 75.5nW /m 2We calculate the electric field intensity using Eq. (1-2):ES 75.5 10 9376.7 5333 V /m Although gain is usually relative to an isotropic antenna, some antenna gains are referred to a λ /2 dipole with an isotropic gain of 2.14 dB.If we approximate the antenna as a point source, we compute the electric field radiated by using Eq. (1.2):e jkRP 0GR4 This requires only that the antenna be small compared to the radial distance R. Equation (1.4) ignores the direction of the electric field, which we define as polarization. The units of the electric field are volts/meter. We determine the far-field pattern by multiplying Eq. (1.4) by R and removing the phase term e jkRsince phase has meaning only when referred to another point in the far field. The far-field electric field E ff unit is volts:During analysis, we often normalize input power to 1 W and can compute gain easily from the electric field by multiplying by a constant 4 = 0.1826374.1.3 EFFECTIVE AREAAntennas capture power from passing waves and deliver some of it to the terminals. Given the power density of the incident wave and the effective area of the antenna, the power 4 108m 2(1.4)E ffP 0G or G 1 E ff P 0 (1.5)delivered to the terminals is the product.(1.6)For an aperture antenna such as a horn, parabolic reflector, or flat-plate array, effective area is physical area multiplied by aperture efficiency. In general, losses due to material, distribution, and mismatch reduce the ratio of the effective area to the physical area. Typical estimatedaperture efficiency for a parabolic reflector is 55%. Even antennas with infinitesimal physical areas, such as dipoles, have effective areas because they remove power from passing waves.1.4 PATH LOSSWe combine the gain of the transmitting antenna with the effective area of the receivingantenna to determine delivered power and path loss. The power density at the receivingantenna is given by Eq. (1.3), and the received power is given by Eq. (1.6). By combining the two, we obtain the path loss:P d A 2G 1 ,P t 4 R 2Antenna 1 transmits, and antenna 2 receives. If the materials in the antennas are linearand isotropic, the transmitting and receiving patterns are identical (reciprocal) [2, p. 116]. When we consider antenna 2 as the transmitting antenna and antenna 1 as the receivingantenna, the path loss isP d A 1G 2 , 2 P t4 R 2Since the responses are reciprocal, the path losses are equal and we can gather and eliminate terms:G 1 G 2= constantA 1 A 2 Because the antennas were arbitrary, this quotient must equal a constant. This constant was found by considering the radiation between two large apertures [3]:(1.7)We substitute this equation into path loss to express it in terms of the gains or effective areas:P d GG 2A 1A 2 P t G 1G 2 4 R 2R 2P d SA eff(1.8)We make quick evaluations of path loss for various units of distance R and for frequency f in megahertz using the formula. path loss(dB)=K U 20log fR G 1 dB G 2 dB (1.9) where Ku depends on the length units:Example Compute the gain of a 3-m-diameter parabolic reflector at 4 GHz assuming 55% aperture efficiency.Gain is related to effective area by Eq. (1.7):4A2 We calculate the area of a circular aperture byA 2 D/2 . By combining these equations,we have Df c where D is the diameter and a is the aperture efficiency. On substituting the values above, we obtain the gain: 923 4 109G 9 0.55 8685 (39.4dB) 0.3 10 G D 2 a a (1.10) Example Calculate the path loss of a 50-km communication link at 2.2 GHz using a transmitter antenna with a gain of 25 dB and a receiver antenna with a gain of 20 dB. Path loss = 32.45 + 20 log[2200(50)] - 25 - 20 = 88.3 dBWhat happens to transmission between two apertures as the frequency is increased? If we assume that the effective area remains constant, as in a parabolic reflector, the transmission increases as the square of frequency: P d A 1A 2 1 P t R 2 2 A 1A 2 f 2 R 2Bf 2where B is a constant for a fixed range. The receiving aperture captures the same power regardless of frequency, but the gain of the transmitting antenna increases as the square of frequency. Hence, the received power also increases as frequency squared. Only for antennas, whose gain is a fixed value when frequency changes, does the path loss increase as the square of frequency.1.5 RADAR RANGE EQUATION AND CROSS SECTIONRadar operates using a double path loss. The radar transmitting antenna radiates a field that illuminates a target. These incident fields excite surface currents that also radiate to produce a second field. These fields propagate to the receiving antenna, where they arecollected. Most radars use the same antenna both to transmit the field and to collect the signal returned, called a monostatic system, whereas we use separate antennas for bistatic radar. The receiving system cannot be detected in a bistatic system because it does not transmit and has greater survivability in a military application.We determine the power density illuminating the target at a rangeR T by using Eq. (1.2):The target ' s radar creocstsio sn (RCS), the scattering area of the object, is expressed in square2meters or dB m : 10 log(square meters). The RCS depends on both the incident and reflected wave directions. We multiply the power collected by the target with its receiving pattern by the gain of the effective antenna due to the currents induced:In a communication system we call Ps the equivalent isotropic radiated power (EIRP), which equals the product of the input power and the antenna gain. The target becomes thetransmitting source and we apply Eq. (1.2) to find the power density at the receiving antenna at a range R R from the target. Finally, the receiving antenna collects the power density with (1.11)S inc P T G T4 R T 2RCS power reflected P s r , r , i , ipowerdensityincident P T G T 4 R T 2 (1.12)an effective areaA R . We combine these ideas to obtain the power delivered to the receiver: We apply Eq. (1.7) to eliminate the effective area of the receiving antenna and gather terms to determine the bistatic radar range equation:P rec G T G Rr , r , i , i P T 4 3 R T 2R R 2 We reduce Eq. (1.13) and collect terms for monostatic radar, where the same antenna is used for both transmitting and receiving:42 Radar received power is proportional to 1/Rand to G . We find the approximate RCS of a flat plate by considering the plate as an antenna with an effective area. Equation (1.11) gives the power density incident on the plate that collects this power over an areaA R :The power scattered by the plate is the power collected,P C , times the gain of the plate as an antenna,G P :This scattered power is the effective radiated power in a particular direction, which in an antenna is the product of the input power and the gain in a particular direction. We calculate the plate gain by using the effective area and find the scattered power in terms of area:P P T G T 4 A RP s 4 R T 2 2We determine the RCS σ Ebqy . (1 .12), the scattered power divided by the incident power density:22P s 4 A R G R i , i G R r , r (1.14)P T G T s 4 R T 2 2 R R i i 4R r r (1.14)The right expression of Eq. (1.14) divides the gain into two pieces for bistatic scattering, where the scattered direction is different from the incident direction. Monostatic scattering uses the same incident and reflected directions. We can substitute any object for the flat plate and use the idea of an effective area and its associated antenna gain. An antenna is an objectP rec S R A RA R P T G T4 R T 2 4 R R 2(1.13)P rec G 2 2P T344 3 R 4 P CP T G T , 4 R T 2 A RP s P C G PP T G T i , i 4 R T 2 A R G P rrwith a unique RCS characteristic because part of the power received will be delivered to the antenna terminals. If we provide a good impedance match to this signal, it will not reradiate and the RCS is reduced. When we illuminate an antenna from an arbitrary direction, some of the incident power density will be scattered by the structure and not delivered to the antenna terminals. This leads to the division of antenna RCS into the antenna mode of reradiated signals caused by terminal mismatch and the structural mode, the fields reflected off the structure for incident power density not delivered to the terminals.1.6WHY USE AN ANTENNA?We use antennas to transfer signals when no other way is possible, such ascommunication with a missile or over rugged mountain terrain. Cables are expensive and take a long time to install. Are there times when we would use antennas over level ground? The large path losses of antenna systems lead us to believe that cable runs are better.中文译文:天线的性能天线的方法一书是从天线辐射的讨论开始。
2011年技术物理学院08级(激光方向)专业英语翻译重点!!!作者:邵晨宇Electromagnetic电磁的principle原则principal主要的macroscopic宏观的microscopic微观的differential微分vector矢量scalar标量permittivity介电常数photons光子oscillation振动density of states态密度dimensionality维数transverse wave横波dipole moment偶极矩diode 二极管mono-chromatic单色temporal时间的spatial空间的velocity速度wave packet波包be perpendicular to线垂直be nomal to线面垂直isotropic各向同性的anistropic各向异性的vacuum真空assumption假设semiconductor半导体nonmagnetic非磁性的considerable大量的ultraviolet紫外的diamagnetic抗磁的paramagnetic顺磁的antiparamagnetic反铁磁的ferro-magnetic铁磁的negligible可忽略的conductivity电导率intrinsic本征的inequality不等式infrared红外的weakly doped弱掺杂heavily doped重掺杂a second derivative in time对时间二阶导数vanish消失tensor张量refractive index折射率crucial主要的quantum mechanics 量子力学transition probability跃迁几率delve研究infinite无限的relevant相关的thermodynamic equilibrium热力学平衡(动态热平衡)fermions费米子bosons波色子potential barrier势垒standing wave驻波travelling wave行波degeneracy简并converge收敛diverge发散phonons声子singularity奇点(奇异值)vector potential向量式partical-wave dualism波粒二象性homogeneous均匀的elliptic椭圆的reasonable公平的合理的reflector反射器characteristic特性prerequisite必要条件quadratic二次的predominantly最重要的gaussian beams高斯光束azimuth方位角evolve推到spot size光斑尺寸radius of curvature曲率半径convention管理hyperbole双曲线hyperboloid双曲面radii半径asymptote渐近线apex顶点rigorous精确地manifestation体现表明wave diffraction波衍射aperture孔径complex beam radius复光束半径lenslike medium类透镜介质be adjacent to与之相邻confocal beam共焦光束a unity determinant单位行列式waveguide波导illustration说明induction归纳symmetric 对称的steady-state稳态be consistent with与之一致solid curves实线dashed curves虚线be identical to相同eigenvalue本征值noteworthy关注的counteract抵消reinforce加强the modal dispersion模式色散the group velocity dispersion群速度色散channel波段repetition rate重复率overlap重叠intuition直觉material dispersion材料色散information capacity信息量feed into 注入derive from由之产生semi-intuitive半直觉intermode mixing模式混合pulse duration脉宽mechanism原理dissipate损耗designate by命名为to a large extent在很大程度上etalon 标准具archetype圆形interferometer干涉计be attributed to归因于roundtrip一个往返infinite geometric progression无穷几何级数conservation of energy能量守恒free spectral range自由光谱区reflection coefficient(fraction of the intensity reflected)反射系数transmission coefficient(fraction of the intensity transmitted)透射系数optical resonator光学谐振腔unity 归一optical spectrum analyzer光谱分析grequency separations频率间隔scanning interferometer扫描干涉仪sweep移动replica复制品ambiguity不确定simultaneous同步的longitudinal laser mode纵模denominator分母finesse精细度the limiting resolution极限分辨率the width of a transmission bandpass透射带宽collimated beam线性光束noncollimated beam非线性光束transient condition瞬态情况spherical mirror 球面镜locus(loci)轨迹exponential factor指数因子radian弧度configuration不举intercept截断back and forth反复spatical mode空间模式algebra代数in practice在实际中symmetrical对称的a symmetrical conforal resonator对称共焦谐振腔criteria准则concentric同心的biperiodic lens sequence双周期透镜组序列stable solution稳态解equivalent lens等效透镜verge 边缘self-consistent自洽reference plane参考平面off-axis离轴shaded area阴影区clear area空白区perturbation扰动evolution渐变decay减弱unimodual matrix单位矩阵discrepancy相位差longitudinal mode index纵模指数resonance共振quantum electronics量子电子学phenomenon现象exploit利用spontaneous emission自发辐射initial初始的thermodynamic热力学inphase同相位的population inversion粒子数反转transparent透明的threshold阈值predominate over占主导地位的monochromaticity单色性spatical and temporal coherence时空相干性by virtue of利用directionality方向性superposition叠加pump rate泵浦速率shunt分流corona breakdown电晕击穿audacity畅通无阻versatile用途广泛的photoelectric effect光电效应quantum detector 量子探测器quantum efficiency量子效率vacuum photodiode真空光电二极管photoelectric work function光电功函数cathode阴极anode阳极formidable苛刻的恶光的irrespective无关的impinge撞击in turn依次capacitance电容photomultiplier光电信增管photoconductor光敏电阻junction photodiode结型光电二极管avalanche photodiode雪崩二极管shot noise 散粒噪声thermal noise热噪声1.In this chapter we consider Maxwell’s equations and what they reveal about the propagation of light in vacuum and in matter. We introduce the concept of photons and present their density of states.Since the density of states is a rather important property,not only for photons,we approach this quantity in a rather general way. We will use the density of states later also for other(quasi-) particles including systems of reduced dimensionality.In addition,we introduce the occupation probability of these states for various groups of particles.在本章中,我们讨论麦克斯韦方程和他们显示的有关光在真空中传播的问题。
麦克斯韦方程组英文表述
麦克斯韦方程组(Maxwell's equations)是电磁理论的基础,描述了电磁场的行为和相互关系。
以下是麦克斯韦方程组的英文表述:
1. Gauss's law for electric fields:
∇·E = ρ/ε₀
2. Gauss's law for magnetic fields:
∇·B = 0
3. Faraday's law of electromagnetic induction:
∇×E = -∂B/∂t
4. Ampère's law with Maxwell's addition:
∇×B = μ₀J + μ₀ε₀∂E/∂t
其中,E表示电场,B表示磁场,ρ表示电荷密度,J表示电流密度,ε₀表示真空介电常数,μ₀表示真空磁导率,∇表示梯度运算符,∂表示偏导数,t表示时间。
这四个方程描述了电荷和电流如何生成和影响电磁场,以及电磁场如何相互作用和传播。
麦克斯韦方程组是电磁学和电磁波理论的基础,对现代科学和工程领域有着广泛的应用。
CHAPTER 2BASIC PLASMA EQUATIONS AND EQUILIBRIUM2.1INTRODUCTIONThe plasma medium is complicated in that the charged particles are both affected by external electric and magnetic fields and contribute to them.The resulting self-consistent system is nonlinear and very difficult to analyze.Furthermore,the inter-particle collisions,although also electromagnetic in character,occur on space and time scales that are usually much shorter than those of the applied fields or the fields due to the average motion of the particles.To make progress with such a complicated system,various simplifying approxi-mations are needed.The interparticle collisions are considered independently of the larger scale fields to determine an equilibrium distribution of the charged-particle velocities.The velocity distribution is averaged over velocities to obtain the macro-scopic motion.The macroscopic motion takes place in external applied fields and in the macroscopic fields generated by the average particle motion.These self-consistent fields are nonlinear,but may be linearized in some situations,particularly when dealing with waves in plasmas.The effect of spatial variation of the distri-bution function leads to pressure forces in the macroscopic equations.The collisions manifest themselves in particle generation and loss processes,as an average friction force between different particle species,and in energy exchanges among species.In this chapter,we consider the basic equations that govern the plasma medium,con-centrating attention on the macroscopic system.The complete derivation of these 23Principles of Plasma Discharges and Materials Processing ,by M.A.Lieberman and A.J.Lichtenberg.ISBN 0-471-72001-1Copyright #2005John Wiley &Sons,Inc.equations,from fundamental principles,is beyond the scope of the text.We shall make the equations plausible and,in the easier instances,supply some derivations in appendices.For the reader interested in more rigorous treatment,references to the literature will be given.In Section2.2,we introduce the macroscopicfield equations and the current and voltage.In Section2.3,we introduce the fundamental equation of plasma physics, for the evolution of the particle distribution function,in a form most applicable for weakly ionized plasmas.We then define the macroscopic quantities and indicate how the macroscopic equations are obtained by taking moments of the fundamental equation.References given in the text can be consulted for more details of the aver-aging procedure.Although the macroscopic equations depend on the equilibrium distribution,their form is independent of the equilibrium.To solve the equations for particular problems the equilibrium must be known.In Section2.4,we introduce the equilibrium distribution and obtain some consequences arising from it and from thefield equations.The form of the equilibrium distribution will be shown to be a consequence of the interparticle collisions,in Appendix B.2.2FIELD EQUATIONS,CURRENT,AND VOLTAGEMaxwell’s EquationsThe usual macroscopic form of Maxwell’s equations arerÂE¼Àm0@H@t(2:2:1)rÂH¼e0@E@tþJ(2:2:2)e0rÁE¼r(2:2:3) andmrÁH¼0(2:2:4) where E(r,t)and H(r,t)are the electric and magneticfield vectors and wherem 0¼4pÂ10À7H/m and e0%8:854Â10À12F/m are the permeability and per-mittivity of free space.The sources of thefields,the charge density r(r,t)and the current density J(r,t),are related by the charge continuity equation(Problem2.1):@rþrÁJ¼0(2:2:5) In general,J¼J condþJ polþJ mag24BASIC PLASMA EQUATIONS AND EQUILIBRIUMwhere the conduction current density J cond is due to the motion of the free charges, the polarization current density J pol is due to the motion of bound charges in a dielectric material,and the magnetization current density J mag is due to the magnetic moments in a magnetic material.In a plasma in vacuum,J pol and J mag are zero and J¼J cond.If(2.2.3)is integrated over a volume V,enclosed by a surface S,then we obtain its integral form,Gauss’law:e0þSEÁd A¼q(2:2:6)where q is the total charge inside the volume.Similarly,integrating(2.2.5),we obtaind q d t þþSJÁd A¼0which states that the rate of increase of charge inside V is supplied by the total currentflowing across S into V,that is,that charge is conserved.In(2.2.2),thefirst term on the RHS is the displacement current densityflowing in the vacuum,and the second term is the conduction current density due to the free charges.We can introduce the total current densityJ T¼e0@E@tþJ(2:2:7)and taking the divergence of(2.2.2),we see thatrÁJ T¼0(2:2:8)In one dimension,this reduces to d J T x=d x¼0,such that J T x¼J T x(t),independent of x.Hence,for example,the total currentflowing across a spatially nonuniform one-dimensional discharge is independent of x,as illustrated in Figure2.1.A generalization of this result is Kirchhoff’s current law,which states that the sum of the currents entering a node,where many current-carrying conductors meet,is zero.This is also shown in Figure2.1,where I rf¼I TþI1.If the time variation of the magneticfield is negligible,as is often the case in plasmas,then from Maxwell’s equations rÂE%0.Since the curl of a gradient is zero,this implies that the electricfield can be derived from the gradient of a scalar potential,E¼Àr F(2:2:9)2.2FIELD EQUATIONS,CURRENT,AND VOLTAGE25Integrating (2.2.9)around any closed loop C givesþC E Ád ‘¼ÀþC r F Ád ‘¼ÀþC d F ¼0(2:2:10)Hence,we obtain Kirchhoff’s voltage law ,which states that the sum of the voltages around any loop is zero.This is illustrated in Figure 2.1,for which we obtainV rf ¼V 1þV 2þV 3that is,the source voltage V rf is equal to the sum of the voltages V 1and V 3across the two sheaths and the voltage V 2across the bulk plasma.Note that currents and vol-tages can have positive or negative values;the directions for which their values are designated as positive must be specified,as shown in the figure.If (2.2.9)is substituted in (2.2.3),we obtainr 2F ¼Àre 0(2:2:11)Equation (2.2.11),Poisson’s equation ,is one of the fundamental equations that we shall use.As an example of its application,consider the potential in the center (x ¼0)of two grounded (F ¼0)plates separated by a distance l ¼10cm and con-taining a uniform ion density n i ¼1010cm 23,without the presence of neutralizing electrons.Integrating Poisson’s equationd 2F d x 2¼Àen i eFIGURE 2.1.Kirchhoff’s circuit laws:The total current J T flowing across a nonuniform one-dimensional discharge is independent of x ;the sum of the currents entering a node is zero (I rf ¼I T þI 1);the sum of voltages around a loop is zero (V rf ¼V 1þV 2þV 3).26BASIC PLASMA EQUATIONS AND EQUILIBRIUMusing the boundary conditions that F ¼0at x ¼+l =2and that d F =d x ¼0at x ¼0(by symmetry),we obtainF ¼12en i e 0l 22Àx 2"#The maximum potential in the center is 2.3Â105V,which is impossibly large for a real discharge.Hence,the ions must be mostly neutralized by electrons,leading to a quasi-neutral plasma.Figure 2.2shows a PIC simulation time history over 10210s of (a )the v x –x phase space,(b )the number N of sheets versus time,and (c )the potential F versus x for 100unneutralized ion sheets (with e /M for argon ions).We see the ion acceleration in (a ),the loss of ions in (b ),and the parabolic potential profile in (c );the maximum potential decreases as ions are lost from the system.We consider quasi-neutrality further in Section 2.4.Electric and magnetic fields exert forces on charged particles given by the Lorentz force law :F ¼q (E þv ÂB )(2:2:12)FIGURE 2.2.PIC simulation of ion loss in a plasma containing ions only:(a )v x –x ion phase space,showing the ion acceleration trajectories;(b )number N of ion sheets versus t ,with the steps indicating the loss of a single sheet;(c )the potential F versus x during the first 10210s of ion loss.2.2FIELD EQUATIONS,CURRENT,AND VOLTAGE 2728BASIC PLASMA EQUATIONS AND EQUILIBRIUMwhere v is the particle velocity and B¼m0H is the magnetic induction vector.The charged particles move under the action of the Lorentz force.The moving charges in turn contribute to both r and J in the plasma.If r and J are linearly related to E and B,then thefield equations are linear.As we shall see,this is not generally the case for a plasma.Nevertheless,linearization may be possible in some cases for which the plasma may be considered to have an effective dielectric constant;that is,the “free charges”play the same role as“bound charges”in a dielectric.We consider this further in Chapter4.2.3THE CONSERVATION EQUATIONSBoltzmann’s EquationFor a given species,we introduce a distribution function f(r,v,t)in the six-dimensional phase space(r,v)of particle positions and velocities,with the interpret-ation thatf(r,v,t)d3r d3v¼number of particles inside a six-dimensional phasespace volume d3r d3v at(r,v)at time tThe six coordinates(r,v)are considered to be independent variables.We illus-trate the definition of f and its phase space in one dimension in Figure2.3.As particles drift in phase space or move under the action of macroscopic forces, theyflow into or out of thefixed volume d x d v x.Hence the distribution functionaf should obey a continuity equation which can be derived as follows.InFIGURE2.3.One-dimensional v x–x phase space,illustrating the derivation of the Boltzmann equation and the change in f due to collisions.time d t,f(x,v x,t)d x a x(x,v x,t)d t particlesflow into d x d v x across face1f(x,v xþd v x,t)d x a x(x,v xþd v x,t)d t particlesflow out of d x d v x across face2 f(x,v x,t)d v x v x d t particlesflow into d x d v x across face3f(xþd x,v x,t)d v x v x d t particlesflow out of d x d v x across face4where a x v d v x=d t and v x;d x=d t are theflow velocities in the v x and x directions, respectively.Hencef(x,v x,tþd t)d x d v xÀf(x,v x,t)d x d v x¼½f(x,v x,t)a x(x,v x,t)Àf(x,v xþd v x,t)a x(x,v xþd v x,t) d x d tþ½f(x,v x,t)v xÀf(xþd x,v x,t)v x d v x d tDividing by d x d v x d t,we obtain@f @t ¼À@@x(f v x)À@@v x(fa x)(2:3:1)Noting that v x is independent of x and assuming that the acceleration a x¼F x=m of the particles does not depend on v x,then(2.3.1)can be rewritten as@f @t þv x@f@xþa x@f@v x¼0The three-dimensional generalization,@f@tþvÁr r fþaÁr v f¼0(2:3:2)with r r¼(^x@=@xþ^y@=@yþ^z@=@z)and r v¼(^x@=@v xþ^y@=@v yþ^z@=@v z)is called the collisionless Boltzmann equation or Vlasov equation.In addition toflows into or out of the volume across the faces,particles can “suddenly”appear in or disappear from the volume due to very short time scale interparticle collisions,which are assumed to occur on a timescale shorter than the evolution time of f in(2.3.2).Such collisions can practically instantaneously change the velocity(but not the position)of a particle.Examples of particles sud-denly appearing or disappearing are shown in Figure2.3.We account for this effect,which changes f,by adding a“collision term”to the right-hand side of (2.3.2),thus obtaining the Boltzmann equation:@f @t þvÁr r fþFmÁr v f¼@f@tc(2:3:3)2.3THE CONSERVATION EQUATIONS29The collision term in integral form will be derived in Appendix B.The preceding heuristic derivation of the Boltzmann equation can be made rigorous from various points of view,and the interested reader is referred to texts on plasma theory, such as Holt and Haskel(1965).A kinetic theory of discharges,accounting for non-Maxwellian particle distributions,must be based on solutions of the Boltzmann equation.We give an introduction to this analysis in Chapter18. Macroscopic QuantitiesThe complexity of the dynamical equations is greatly reduced by averaging over the velocity coordinates of the distribution function to obtain equations depending on the spatial coordinates and the time only.The averaged quantities,such as species density,mean velocity,and energy density are called macroscopic quantities,and the equations describing them are the macroscopic conservation equations.To obtain these averaged quantities we take velocity moments of the distribution func-tion,and the equations are obtained from the moments of the Boltzmann equation.The average quantities that we are concerned with are the particle density,n(r,t)¼ðf d3v(2:3:4)the particlefluxG(r,t)¼n u¼ðv f d3v(2:3:5)where u(r,t)is the mean velocity,and the particle kinetic energy per unit volumew¼32pþ12mu2n¼12mðv2f d3v(2:3:6)where p(r,t)is the isotropic pressure,which we define below.In this form,w is sumof the internal energy density32p and theflow energy density12mu2n.Particle ConservationThe lowest moment of the Boltzmann equation is obtained by integrating all terms of(2.3.3)over velocity space.The integration yields the macroscopic continuity equation:@n@tþrÁ(n u)¼GÀL(2:3:7)The collision term in(2.3.3),which yields the right-hand side of(2.3.7),is equal to zero when integrated over velocities,except for collisions that create or destroy 30BASIC PLASMA EQUATIONS AND EQUILIBRIUMparticles,designated as G and L ,respectively (e.g.,ionization,recombination).In fact,(2.3.7)is transparent since it physically describes the conservation of particles.If (2.3.7)is integrated over a volume V bounded by a closed surface S ,then (2.3.7)states that the net number of particles generated per second within V ,either flows across the surface S or increases the number of particles within V .For common low-pressure discharges in the steady state,G is usually due to ioniz-ation by electron–neutral collisions:G ¼n iz n ewhere n iz is the ionization frequency.The volume loss rate L ,usually due to recom-bination,is often negligible.Hencer Á(n u )¼n iz n e (2:3:8)in a typical discharge.However,note that the continuity equation is clearly not sufficient to give the evolution of the density n ,since it involves another quantity,the mean particle velocity u .Momentum ConservationTo obtain an equation for u ,a first moment is formed by multiplying the Boltzmann equation by v and integrating over velocity.The details are complicated and involve evaluation of tensor elements.The calculation can be found in most plasma theory texts,for example,Krall and Trivelpiece (1973).The result is mn @u @t þu Ár ðÞu !¼qn E þu ÂB ðÞÀr ÁP þf c (2:3:9)The left-hand side is the species mass density times the convective derivative of the mean velocity,representing the mass density times the acceleration.The convective derivative has two terms:the first term @u =@t represents an acceleration due to an explicitly time-varying u ;the second “inertial”term (u Ár )u represents an acceleration even for a steady fluid flow (@=@t ;0)having a spatially varying u .For example,if u ¼^xu x (x )increases along x ,then the fluid is accelerating along x (Problem 2.4).This second term is nonlinear in u and can often be neglected in discharge analysis.The mass times acceleration is acted upon,on the right-hand side,by the body forces,with the first term being the electric and magnetic force densities.The second term is the force density due to the divergence of the pressure tensor,which arises due to the integration over velocitiesP ij ¼mn k v i Àu ðÞv j Àu ÀÁl v (2:3:10)2.3THE CONSERVATION EQUATIONS 31where the subscripts i,j give the component directions and kÁl v denotes the velocity average of the bracketed quantity over f.ÃFor weakly ionized plasmas it is almost never used in this form,but rather an isotropic version is employed:P¼p000p000p@1A(2:3:11)such thatrÁP¼r p(2:3:12) a pressure gradient,withp¼13mn k(vÀu)2l v(2:3:13)being the scalar pressure.Physically,the pressure gradient force density arises as illustrated in Figure2.4,which shows a small volume acted upon by a pressure that is an increasing function of x.The net force on this volume is p(x)d AÀp(xþd x)d A and the volume is d A d x.Hence the force per unit volume isÀ@p=@x.The third term on the right in(2.3.9)represents the time rate of momentum trans-fer per unit volume due to collisions with other species.For electrons or positive ions the most important transfer is often due to collisions with neutrals.The transfer is usually approximated by a Krook collision operatorf j c¼ÀXbmn n m b(uÀu b):Àm(uÀu G)Gþm(uÀu L)L(2:3:14)where the summation is over all other species,u b is the mean velocity of species b, n m b is the momentum transfer frequency for collisions with species b,and u G and u L are the mean velocities of newly created and lost particles.Generally j u G j(j u j for pair creation by ionization,and u L%u for recombination or charge transfer lossprocesses.We discuss the Krook form of the collision operator further in Chapter 18.The last two terms in(2.3.14)are generally small and give the momentum trans-fer due to the creation or destruction of particles.For example,if ions are created at rest,then they exert a drag force on the moving ionfluid because they act to lower the averagefluid velocity.A common form of the average force(momentum conservation)equation is obtained from(2.3.9)neglecting the magnetic forces and taking u b¼0in theÃWe assume f is normalized so that k f lv ¼1.32BASIC PLASMA EQUATIONS AND EQUILIBRIUMKrook collision term for collisions with one neutral species.The result is mn @u @t þu Ár u !¼qn E Àr p Àmn n m u (2:3:15)where only the acceleration (@u =@t ),inertial (u Ár u ),electric field,pressure gradi-ent,and collision terms appear.For slow time variation,the acceleration term can be neglected.For high pressures,the inertial term is small compared to the collision term and can also be dropped.Equations (2.3.7)and (2.3.9)together still do not form a closed set,since the pressure tensor P (or scalar pressure p )is not determined.The usual procedure to close the equations is to use a thermodynamic equation of state to relate p to n .The isothermal relation for an equilibrium Maxwellian distribution isp ¼nkT(2:3:16)so thatr p ¼kT r n (2:3:17)where T is the temperature in kelvin and k is Boltzmann’s constant (k ¼1.381Â10223J /K).This holds for slow time variations,where temperatures are allowed to equilibrate.In this case,the fluid can exchange energy with its sur-roundings,and we also require an energy conservation equation (see below)to deter-mine p and T .For a room temperature (297K)neutral gas having density n g and pressure p ,(2.3.16)yieldsn g (cm À3)%3:250Â1016p (Torr)(2:3:18)p FIGURE 2.4.The force density due to the pressure gradient.2.3THE CONSERVATION EQUATIONS 33Alternatively,the adiabatic equation of state isp¼Cn g(2:3:19) such thatr p p ¼gr nn(2:3:20)where g is the ratio of specific heat at constant pressure to that at constant volume.The specific heats are defined in Section7.2;g¼5/3for a perfect gas; for one-dimensional adiabatic motion,g¼3.The adiabatic relation holds for fast time variations,such as in waves,when thefluid does not exchange energy with its surroundings;hence an energy conservation equation is not required. For almost all applications to discharge analysis,we use the isothermal equation of state.Energy ConservationThe energy conservation equation is obtained by multiplying the Boltzmannequation by12m v2and integrating over velocity.The integration and some othermanipulation yield@ @t32pþrÁ32p uðÞþp rÁuþrÁq¼@@t32pc(2:3:21)Here32p is the thermal energy density(J/m3),32p u is the macroscopic thermal energyflux(W/m2),representing theflow of the thermal energy density at thefluid velocityu,p rÁu(W/m3)gives the heating or cooling of thefluid due to compression orexpansion of its volume(Problem2.5),q is the heatflow vector(W/m2),whichgives the microscopic thermal energyflux,and the collisional term includes all col-lisional processes that change the thermal energy density.These include ionization,excitation,elastic scattering,and frictional(ohmic)heating.The equation is usuallyclosed by setting q¼0or by letting q¼Àk T r T,where k T is the thermal conduc-tivity.For most steady-state discharges the macroscopic thermal energyflux isbalanced against the collisional processes,giving the simpler equationrÁ32p u¼@32pc(2:3:22)Equation(2.3.22),together with the continuity equation(2.3.8),will often prove suf-ficient for our analysis.34BASIC PLASMA EQUATIONS AND EQUILIBRIUMSummarySummarizing our results for the macroscopic equations describing the electron and ionfluids,we have in their most usually used forms the continuity equationrÁ(n u)¼n iz n e(2:3:8) the force equation,mn @u@tþuÁr u!¼qn EÀr pÀmn n m u(2:3:15)the isothermal equation of statep¼nkT(2:3:16) and the energy-conservation equationrÁ32p u¼@@t32pc(2:3:22)These equations hold for each charged species,with the total charges and currents summed in Maxwell’s equations.For example,with electrons and one positive ion species with charge Ze,we haver¼e Zn iÀn eðÞ(2:3:23)J¼e Zn i u iÀn e u eðÞ(2:3:24)These equations are still very difficult to solve without simplifications.They consist of18unknown quantities n i,n e,p i,p e,T i,T e,u i,u e,E,and B,with the vectors each counting for three.Various simplifications used to make the solutions to the equations tractable will be employed as the individual problems allow.2.4EQUILIBRIUM PROPERTIESElectrons are generally in near-thermal equilibrium at temperature T e in discharges, whereas positive ions are almost never in thermal equilibrium.Neutral gas mol-ecules may or may not be in thermal equilibrium,depending on the generation and loss processes.For a single species in thermal equilibrium with itself(e.g.,elec-trons),in the absence of time variation,spatial gradients,and accelerations,the2.4EQUILIBRIUM PROPERTIES35Boltzmann equation(2.3.3)reduces to@f @tc¼0(2:4:1)where the subscript c here represents the collisions of a particle species with itself. We show in Appendix B that the solution of(2.4.1)has a Gaussian speed distribution of the formf(v)¼C eÀj2m v2(2:4:2) The two constants C and j can be obtained by using the thermodynamic relationw¼12mn k v2l v¼32nkT(2:4:3)that is,that the average energy of a particle is12kT per translational degree offreedom,and by using a suitable normalization of the distribution.Normalizing f(v)to n,we obtainCð2p0d fðpsin u d uð1expÀj2m v2ÀÁv2d v¼n(2:4:4)and using(2.4.3),we obtain1 2mCð2pd fðpsin u d uð1expÀj2m v2ÀÁv4d v¼32nkT(2:4:5)where we have written the integrals over velocity space in spherical coordinates.The angle integrals yield the factor4p.The v integrals are evaluated using the relationÃð10eÀu2u2i d u¼(2iÀ1)!!2ffiffiffiffipp,where i is an integer!1:(2:4:6)Solving for C and j we havef(v)¼nm2p kT3=2expÀm v22kT(2:4:7)which is the Maxwellian distribution.Ã!!denotes the double factorial function;for example,7!!¼7Â5Â3Â1. 36BASIC PLASMA EQUATIONS AND EQUILIBRIUMSimilarly,other averages can be performed.The average speed vis given by v ¼m =2p kT ðÞ3=2ð10v exp Àv 22v 2th !4p v 2d v (2:4:8)where v th ¼(kT =m )1=2is the thermal velocity.We obtainv ¼8kT p m 1=2(2:4:9)The directed flux G z in (say)the þz direction is given by n k v z l v ,where the average is taken over v z .0only.Writing v z ¼v cos u we have in spherical coordinatesG z ¼n m 2p kT 3=2ð2p 0d f ðp =20sin u d u ð10v cos u exp Àv 22v 2th v 2d v Evaluating the integrals,we findG z ¼14n v (2:4:10)G z is the number of particles per square meter per second crossing the z ¼0surfacein the positive direction.Similarly,the average energy flux S z ¼n k 1m v 2v z l v in theþz direction can be found:S z ¼2kT G z .We see that the average kinetic energy W per particle crossing z ¼0in the positive direction isW ¼2kT (2:4:11)It is sometimes convenient to define the distribution in terms of other variables.For example,we can define a distribution of energies W ¼12m v 2by4p g W ðÞd W ¼4p f v ðÞv 2d vEvaluating d v =d W ,we see that g and f are related byg W ðÞ¼v (W )f ½v (W ) m (2:4:12)where v (W )¼(2W =m )1=2.Boltzmann’s RelationA very important relation can be obtained for the density of electrons in thermal equilibrium at varying positions in a plasma under the action of a spatially varying 2.4EQUILIBRIUM PROPERTIES 3738BASIC PLASMA EQUATIONS AND EQUILIBRIUMpotential.In the absence of electron drifts(u e;0),the inertial,magnetic,and fric-tional forces are zero,and the electron force balance is,from(2.3.15)with@=@t;0,en e Eþr p e¼0(2:4:13) Setting E¼Àr F and assuming p e¼n e kT e,(2.4.13)becomesÀen e r FþkT e r n e¼0or,rearranging,r(e FÀkT e ln n e)¼0(2:4:14) Integrating,we havee FÀkT e ln n e¼constorn e(r)¼n0e e F(r)=kT e(2:4:15)which is Boltzmann’s relation for electrons.We see that electrons are“attracted”to regions of positive potential.We shall generally write Boltzmann’s relation in more convenient unitsn e¼n0e F=T e(2:4:16)where T e is now expressed in volts,as is F.For positive ions in thermal equilibrium at temperature T i,a similar analysis shows thatn i¼n0eÀF=T i(2:4:17) Hence positive ions in thermal equilibrium are“repelled”from regions of positive potential.However,positive ions are almost never in thermal equilibrium in low-pressure discharges because the ion drift velocity u i is large,leading to inertial or frictional forces in(2.3.15)that are comparable to the electricfield or pressure gra-dient forces.Debye LengthThe characteristic length scale in a plasma is the electron Debye length l De.As we will show,the Debye length is the distance scale over which significant charge densities can spontaneously exist.For example,low-voltage(undriven)sheaths are typically a few Debye lengths wide.To determine the Debye length,let us intro-duce a sheet of negative charge having surface charge density r S,0C/m2into an。
maxwell方程的物理意义英语Maxwell's Equations: The Foundation of Electromagnetism.James Clerk Maxwell's equations, published in 1861-1862, are a set of four partial differential equations that describe the behavior of electric and magnetic fields. They are considered one of the most important achievements in physics, as they provide a unified description of electricity, magnetism, and light.Gauss's Law for Electric Fields:The first of Maxwell's equations, Gauss's law forelectric fields, states that the net electric flux through any closed surface is proportional to the charge enclosedby the surface. In other words, the amount of electricfield passing through a surface is directly related to the amount of electric charge inside the surface.Gauss's Law for Magnetic Fields:Gauss's law for magnetic fields, the second equation, states that the net magnetic flux through any closed surface is zero. This means that magnetic field lines always form closed loops and do not have sources or sinks.Faraday's Law of Induction:The third equation, Faraday's law of induction, states that the electromotive force (EMF) around any closed loop is equal to the negative rate of change of magnetic flux through the loop. This law describes the phenomenon of electromagnetic induction, which is the process by which a changing magnetic field induces an electric field.Ampère's Circuital Law with Maxwell's Addition:The fourth equation, Ampère's circuital law with Maxwell's addition, states that the line integral of the magnetic field around any closed loop is equal to the current passing through the loop plus the displacement current. The displacement current term, introduced byMaxwell, accounts for the effects of changing electric fields on magnetic fields.Physical Significance of Maxwell's Equations:Maxwell's equations have profound physical implications that extend beyond their mathematical formulation. They form the basis for understanding a wide range of electromagnetic phenomena, including:Electrostatic phenomena: Gauss's law for electric fields describes the behavior of electric charges at rest, explaining phenomena such as electric fields, electric potential, and capacitance.Magnetostatic phenomena: Gauss's law for magnetic fields describes the behavior of magnetic materials, explaining phenomena such as magnetic fields, magnetic domains, and magnetic poles.Electromagnetic induction: Faraday's law of induction describes the generation of electric fields from changingmagnetic fields, providing the basis for generators, transformers, and inductors.Electromagnetic waves: Ampère's circuital law with Maxwell's addition, when combined with Gauss's laws, predicts the existence of electromagnetic waves that travel at the speed of light. These waves form the basis of light, radio waves, and other forms of electromagnetic radiation.Unification of Electricity and Magnetism:One of the most significant contributions of Maxwell's equations was the unification of electricity and magnetism. Prior to Maxwell, these two phenomena were considered separate entities. Maxwell's equations showed that electricity and magnetism are interconnected and interdependent, forming a single electromagnetic field.Foundation of Modern Physics:Maxwell's equations played a pivotal role in the development of modern physics. They provided thetheoretical framework for Einstein's theory of special relativity, which showed that space and time are not absolute but are intertwined with the electromagnetic field.Technological Applications:Maxwell's equations have had a profound impact on technology. They form the basis for numerous inventions and applications, including:Electric motors and generators: Faraday's law of induction enables the conversion of mechanical energy into electrical energy and vice versa.Transformers: Transformers use the principles of electromagnetic induction to change the voltage and current of alternating current (AC) circuits.Microwaves: Microwaves use electromagnetic waves to heat food by exciting water molecules.Cellular phones: Cellular phones rely onelectromagnetic waves to transmit and receive signals.Conclusion:Maxwell's equations are a cornerstone of modern physics. They provide a comprehensive description of the behavior of electric and magnetic fields and have revolutionized our understanding of electricity, magnetism, and light. Their impact extends far beyond their mathematical formulation, forming the foundation for numerous technological advancements that shape our daily lives.。